We numerically examine the mass transport into a fluid in the classical dri
ven cavity problem and in the limit of large Peclet number, Pe. The species
absorbed into the fluid is allowed to undergo a simple first-order chemica
l reaction. Two particular types of boundary conditions are imposed: a macr
oscopic gradient between the bottom and top surface and a zero-flux conditi
on. We demonstrate that, in the absence of a chemical reaction and when a m
acroscopic gradient is present, mass transport into the liquid is enhanced
due to a recirculation zone in the cavity which is connected to the top and
bottom surfaces through two boundary layers. The corresponding enhancement
is large and scales as Pe(1 2). In the presence of a chemical reaction wit
h rate constant k, adsorption into the liquid is further enhanced with the
flux at the top surface now scaling as k(1 2) for k much greater than Pe, H
owever, for k = O(Pe), the chemical reaction removes the central spatially
uniform concentration region from the cavity as well as the boundary laver
at the bottom wall. (C) 2001 Elsevier Science Ltd. All rights reserved.